Tropical.
Coastal areas tend to have milder temperatures compared to inland regions due to the moderating effect of the ocean. Water heats up and cools down more slowly than land, which means coastal areas experience less temperature fluctuation. Additionally, coastal breezes can bring cooler air from the ocean inland, further reducing temperatures in nearby areas. This results in a generally cooler climate near the coast compared to more extreme temperatures found further inland.
The climate in a hot dry desert is influenced by low moisture levels and high temperatures due to sparse vegetation and lack of rainfall. In contrast, the climate in a hot humid swamp is characterized by high moisture levels and high temperatures due to constant evaporation from water bodies and dense vegetation, leading to high humidity levels and regular rainfall.
Typically, land breezes are cooler than water breezes because land heats up and cools down more quickly than water. This temperature difference creates the conditions for the air to move from the cooler land to the warmer water during a land breeze, and from the cooler water to the warmer land during a sea breeze.
When the sun goes down, the ground starts to cool down. This causes the air above it to also cool, and cooler air tends to sink. As cooler air sinks, it displaces the warmer air, creating a breeze. This breeze can feel cooler because it is coming from an area that has been cooled by the setting sun.
To determine a climate range on a climate graph, you would look at the highest temperature (usually in the summer months) and the lowest temperature (usually in the winter months) plotted on the graph. The difference between these two points gives you the climate range for that location.
Land near the ocean has a milder climate because water heats and cools more slowly than land, creating a moderating effect on temperatures. This results in more stable temperatures throughout the year compared to the extreme temperatures experienced in inland areas. Additionally, oceanic influences such as sea breezes can further contribute to the mild climate near the coast.
Mountain breezes are the breezes in which mountains give off oxygen and carbon to create moisture, then it flows down to the cities causing cold wind. Valley Breezes are the air trapped in the valleys below making its way to the top and spreading out to combine with the mountain breezes.
benefits of economic and it holds wage levels down
wind, breezes, gales, zephyrs, thermals, down drafts !
No toad lives exclusively underground but many species will hibernate or estivate underground. Hibernation is where climate temperatures become unfavorably cold and the species has to shut itself down for prolonged periods of time in order to survive. Estivation is where climate temperatures become unfavorably hot or dry and the species has to shut itself down for prolonged periods of time in order to survive.
Deforestation and pollution have contributed to the climate change in the Amazon. Due to more trees being cut down, rainfall is beginning to decrease while temperatures increase.
A warm and humid climate is most prone to chemical weathering. High temperatures and moisture promote chemical reactions that break down rocks and minerals over time.
Rocks weather fastest in a warm and wet climate because the combination of moisture and high temperatures accelerates chemical reactions that break down the rock.
A fleet of sailboats might make the best of land and sea breezes during the late morning to early afternoon when land heats up and generates a sea breeze, which combines with the prevailing winds for optimal sailing conditions.
In the summer, the sun is present almost 24 hours a day and warms it about 3°C to 12°C. In the winter, the temperatures drop down into extreme cold weather. The average temperatures are -28°C to -70°C.
Land breezes are created at night when the land cools down faster than the sea, causing air to move from the land towards the sea. Sea breezes are created during the day when the land warms up faster than the sea, causing air to move from the sea towards the land. These differences in temperature create variations in air pressure, leading to the movement of air.
Mountain breezes typically form during the night. As the sun sets, the air in the valley cools more quickly than the air on the mountain, creating a temperature difference. This temperature difference causes the air to flow from the mountain down into the valley, creating a mountain breeze.